A Treatise on the Plague and Yellow Fever: With an Appendix, containing histories of the plague at Athens in the time of the Peloponnesian War; at Constantinople in the time of Justinian; at London in 1665; at Marseilles in 1720Tytler, James
History
A Treatise on the Plague and Yellow Fever: With an Appendix, containing histories of the plague at Athens in the time of the Peloponnesian War; at Constantinople in the time of Justinian; at London in 1665; at Marseilles in 1720
Tytler, James
Plague -- Early works to 1800; Yellow fever -- Early works to 1800
The aerial fluid, discovered by Dr. Black, was one of those most
commonly met with. He called it _fixed air_, from its property of
adhering or fixing itself to different bodies. It was found to be the
same with that which had been discovered by Van Helmont, and by him
named _gas sylvestre_ (spirit of wood)[64] or the fume of charcoal;
it was found to be the same with the steam of fermenting liquor, and
with that very frequent and dangerous vapour, met with in coal mines,
called in Scotland the _choke-damp_. Like other discoveries, this was
quickly pushed beyond its proper bounds, and applied to the solution of
phenomena which it could not solve. Dr. MBride, particularly, supposed
it to be the bond of union between the particles of matter, or in other
words the principle of cohesion itself. It was also supposed to be
the substance of those scorching winds, called _samiel_, met with in
Asia and Africa, and which sometimes prove fatal to travellers. The
pernicious vapours called _mofetes_, which sometimes issue from the old
lavas of Vesuvius in Italy, were likewise supposed to be the same;[65]
but of this, particularly with regard to the samiel, there seems to be
no sufficient evidence.
[64] This must be understood only of its general properties and
effects; for, though the fume of charcoal possesses many of the
apparent properties of pure fixed air, it contains also a very
considerable quantity of another kind of gas.
[65] Many fabulous stories have been related concerning the samiel.
Even so late a traveller as Mr. Ives has adopted some of those
exaggerated accounts which have been discredited by those who have
long resided in the countries where this wind is commonly met with.
It is not peculiar to the deserts of Arabia, but is met with in all
hot countries which are destitute of water. In the African deserts
therefore it is common; and Mr. Bruce describes it by the name of
_simoom_. It was preceded by whirlwinds of a very extraordinary
kind. “In that vast expanse of desert (says he) from W. and to N. W.
of us, we saw a number of prodigious pillars of sand at different
distances, at times moving with great celerity, at others walking on
with a majestic slowness. At intervals we thought they were coming
in a very few minutes to overwhelm us; and small quantities of sand
did actually more than once reach us. Again they would retreat so as
to be almost out of sight; their tops reaching to the very clouds.*
There the tops often separated from the bodies; and these, once
disjoined, dispersed in the air, and did not appear more. Sometimes
they were broken near the middle, as if struck with a large cannon
shot. About noon they began to advance with considerable swiftness
upon us, the wind being very strong at north. Eleven of them ranged
along side of us at about the distance of three miles. The largest
of them appeared to me at that distance to be about ten feet
diameter....
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